B107 Lecture Notes - Lecture 8: Karst, Dakota Formation, Vadose Zone

342 views4 pages
8 Apr 2017
Department
Course
Professor

Document Summary

An artesian well occurs in a confined (pressurized) aquifer, where the level of the water in the well rises above the top of the aquifer. When water under pressure rises in wells to a level above the top of the aquifer. Sometimes spouts continuously into air unless it is capped. A hot spring is a spring where water is warmer than human body temperature, while a geyser is a type of near-boiling hot spring that periodically erupts hot water and steam. Karst topography consists of an irregular series of valleys, caves, and sinkholes created by the solution of the underlying limestone bedrock by groundwater. Area with many sinkholes and with cave systems beneath the land surface. A perched water table is caused by a low-permeability geologic material of limited extent within the unsaturated zone that allows a localized mass of groundwater to accumulate above. Top of a body of groundwater separated from main water table beneath it by unsaturated zone.

Get access

Grade+20% off
$8 USD/m$10 USD/m
Billed $96 USD annually
Grade+
Homework Help
Study Guides
Textbook Solutions
Class Notes
Textbook Notes
Booster Class
40 Verified Answers
Class+
$8 USD/m
Billed $96 USD annually
Class+
Homework Help
Study Guides
Textbook Solutions
Class Notes
Textbook Notes
Booster Class
30 Verified Answers

Related Documents